Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
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Page 103
... flysch from the Indus Suture to rest upon the Kailas moved in a reverse sense as did the backward folds and thrusts with a common southward vergence on the Southern Alps in the immediate south of the Insubric Line . This has led Valdiya ...
... flysch from the Indus Suture to rest upon the Kailas moved in a reverse sense as did the backward folds and thrusts with a common southward vergence on the Southern Alps in the immediate south of the Insubric Line . This has led Valdiya ...
Page 104
... Flysch is a subduction complex . It is believed that this flysch was the last filling of the narrowing eugeosyncline , accumulated not long before the closure of the trench in the late Cretaceous . One can visualise further from melange ...
... Flysch is a subduction complex . It is believed that this flysch was the last filling of the narrowing eugeosyncline , accumulated not long before the closure of the trench in the late Cretaceous . One can visualise further from melange ...
Page 106
... Flysch Nappe . Being the last filling of the narrowing Himalayan eugeosyncline , the Indus Flysch would not have been subducted to a depth great enough for it to undergo metamorphism before it was finally everted in nappe form from the ...
... Flysch Nappe . Being the last filling of the narrowing Himalayan eugeosyncline , the Indus Flysch would not have been subducted to a depth great enough for it to undergo metamorphism before it was finally everted in nappe form from the ...
Contents
Tectonics and Structure of the Pamirs | 1 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 17 |
Peninsular and Himalayan Precambrian Belts | 31 |
Copyright | |
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Acharyya Alpine Alps associated basement faults basin batholith belt biotite Bordet Central Crystalline chlorite collision continental Cretaceous crust crustal deformation deposits earthquakes eastern Eocene facies flysch folds foreland formation Gansser Garhwal garnet Geodynamics Geol Geology Geophys geosyncline gneiss Gondwana granite Higher Himalaya Himalaya Indian plate Indian Shield Indus Suture island arc Jour Karakorum Kashmir Klootwijk Krol Kumaun Ladakh Late Lesser Himalaya limestone Lower magmatic Main Boundary Main Central Thrust margin melange Mesozoic metamorphism Molnar movement nappe Nepal northern northward occur oceanic ophiolite orogenic Pakistan Palaeocene palaeomagnetic Palaeozoic Pamir Pande Panjal Permian phase plate tectonics Plateau Precambrian Proterozoic quartzite Quetta Range region rocks rotation Saklani sandstones Saxena schists sedimentary sediments seismicity sequence serpentinite Sharma Shyok Simla Siwalik southern stratigraphic structural Surv suture zone Tectonic Zone Tectonophysics Tertiary Tethyan Tethys thickness Tibet Tibetan slab Triassic Upper Valdiya volcanics